A saponite from Ballarat was intercalated with Al polycations by four
different procedures involving different sources of polycations, and s
tabilised by calcination (pillared). Si-29 and Al-27 solid-state MNR o
f both the intercalated and the pillared samples have been measured an
d are discussed. Si-29 NMR leads us to propose a pillaring mechanism,
involving H+ attack of the clay tetrahedral sheet followed by AlO4 tet
rahedra inversion, similar to that previously proposed for beidellites
. Al-27 NMR reveals that the pillars are not fundamentally modified up
on calcination at 500-degrees-C although they undergo reversible dehyd
ration reactions; at 750-degrees-C and above, a strong pillar reorgani
sation occurs prior to collapse of the global structure.